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dc.contributor.advisorHerbert H. Einstein.en_US
dc.contributor.authorLocsin, Jean Louis Zuñiga, 1975-en_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Civil and Environmental Engineering.en_US
dc.date.accessioned2006-07-31T15:28:47Z
dc.date.available2006-07-31T15:28:47Z
dc.date.copyright2005en_US
dc.date.issued2005en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/33735
dc.descriptionThesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2005.en_US
dc.descriptionIncludes bibliographical references (p. 485-489).en_US
dc.description.abstractRock fracture pattern description is important in civil engineering, engineering geology, and petroleum engineering. Deformability, strength, and stability of a rock mass as well as fluid flow through it are all influenced by fractures. Rock fracture patterns normally cannot be observed completely so different approaches have been used to model them. Geometric models, which use probabilistic processes usually not or only indirectly related to mechanics, are often used for this purpose. Mechanics-based models, on the other hand, can only describe simpler fracture patterns. This research will improve on fracture pattern modeling capabilities, specifically for layer-perpendicular joints in sedimentary rock. Layer-perpendicular joints in sedimentary rock represent relatively simple fracture patterns that are usually confined within a competent layer bounded by ductile non-jointing layers. Field and laboratory studies in the literature suggest that their spacing is related to layer thickness and follows some probability distribution. Laboratory results in the literature also suggest that for a given layer thickness, a limiting joint spacing exists (i.e., joint saturation); this is not apparent in field data.en_US
dc.description.abstract(cont.) Existing models for layer-perpendicular joints in sedimentary rock consider some but not all of these aspects. Two new models are developed to better consider them. The first model (flaw model) is mechanics-based and relies on tensile stress and tensile strength submodels to generate joint patterns. Tensile strength can be correlated or uncorrelated. Compressive stress and interface slip saturation mechanisms are also implemented. The second model (rejection procedure) is a faster and largely probabilistic approach that generates joint patterns from a continuously updated probability density function but this function is assumed to depend only on tensile stress. For this reason, the flaw model must always be used to evaluate rejection procedure results. Only the compressive stress saturation is considered in the rejection procedure. Comparisons with field data indicate that both models can produce realistic joint patterns except where there are through-going joints or where strike varies considerably. Also, results indicate that saturation does not always occur in the field. Additionally, it is found that the use of an uncorrelated submodel in the flaw model is adequate for producing realistic joint patterns.en_US
dc.description.statementofresponsibilityby Jean Louis Zuñiga Locsin.en_US
dc.format.extent539 p.en_US
dc.format.extent25333066 bytes
dc.format.extent25356863 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypeapplication/pdf
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582
dc.subjectCivil and Environmental Engineering.en_US
dc.titleModeling joint patterns using combinations of mechanical and probabilistic conceptsen_US
dc.typeThesisen_US
dc.description.degreePh.D.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineering
dc.identifier.oclc65171046en_US


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